Jun 3 2014
Chalcopyrite is a copper iron sulfide mineral, having a tetragonal crystal system. It was named after the Greek word chalkos, meaning copper, and pyrites, meaning strike fire.
Properties of Chalcopyrite
The following are the key properties of Chalcopyrite:
Elements |
Content 1 |
Content 2 |
Cu |
35.03 |
34.63 |
S |
34.96 |
34.94 |
Fe |
31.00 |
30.43 |
Total |
100.99 |
100.00 |
- Cell Data
- Space Group: I42d
- a = 5.281
- c = 10.401
- Z = 4
- Crystal Data
- Tetragonal
- Point Group: 42m
- Equant, tetrahedral-shaped crystals, may be modified by scalenohedral faces, to as large as 10cm. Sphenoidal faces {112} typically large, dull in luster, and striated k [110]; {112} faces are small and bright. Commonly massive, compact; can be botryoidal
- Twinning: Twin plane {112}, composition surface commonly {112}; twin plane {012}; also by rotation about [001] with composition plane {110}, producing penetration twins
- X-ray Powder Pattern: 3.038 (100), 1.8570 (35), 1.5927 (27), 1.8697 (22), 1.5753 (14), 2.644 (5), 1.2025 (5)
- Estimated Properties
Electron density |
Bulk density (electron density) = 3.98 g/cm3
note: Specific gravity of Chalcopyrite = 4.20 g/cm3 |
Photoelectric |
PEChalcopyrite = 26.59 barns/electron
U = PEChalcopyrite x ρElectron density = 105.88 barns/cm3 |
Fermion index |
Fermion index = 0.0090
Boson index = 0.9909 |
Radioactivity
|
Chalcopyrite is not radioactive
|
How to Identify Chalcopyrite
Chalcopyrite can be identified in the field by its honey-yellow or brass-yellow variations, with a greenish-black streak, and metallic luster. It has an indistinct cleavage, and becomes magnetic after heating. It is non-fluorescent, with opaque properties. Its fractures are brittle, as shown by non-metallic minerals and glasses. It can be formed as euhedral crystals, with striated lines on the crystal face.
The average density of chalcopyrite is 4.19 g/cm3, and its hardness is 3.5.
Global Distribution
Chalcopyrite is distributed in the following places:
- Copper mines of Arizona
- Groundhog mine, Vanadium, Grant Co. New Mexico
- Rossie lead mines, St. Lawrence Co. New York
- Chester Co. Pennsylvania
- Joplin, Jasper Co. Missouri
- Cananea, Sonora, Mexico
- Creek mine, near Timmins, Huaron
- Bansk´a Stiavnica (Schemnitz), Slovakia
- Horn´i Slavkov (Schlaggenwald), Czech Republic
- Freiberg, Saxony
- Dillenburg, Hesse
- Georg mine, near Horhausen, Westerwald
- A number of mines in North Rhine-Westphalia, Germany
- Vinsknoes, Karmoen, Norway
- Ani and Arakawa mines, Akita Prefecture, Japan
- Nababiep mine, Cape Province, South Africa
Occurrence of Chalcopyrite and Useful Mineral Association
Chalcopyrite occurs as a primary mineral in hydrothermal veins, stockworks, disseminations, and massive replacements, or as an ex-solution product in mafic igneous rocks. It can also be found as a sedimentary origin, controlled by redox conditions.
Minerals such as pyrite, tetrahedrite, galena, sphalerite, and some of the copper sulfides, are closely associated with chalcopyrite.
References